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i'•••liDl<br />

Group E: Pure water group<br />

220<br />

(a) Waters usually contain < 150 mg r 1 TDS, but may approach 20 - 40 mg r 1 in the<br />

Pretoria quartzites.<br />

(bl The Si0 2 content is generally high, especially in Old granite waters in the southern<br />

Transvaal. The exception is water from the Table Mountain Series in the Cape<br />

Province which approximates to the slightly saline Group B water.<br />

(c) Moderately low chloride concentrations ranging from 8 -14% are evident, with the<br />

exception <strong>of</strong> waters from the Table Mountain Series in Natal and the Cape<br />

Province, and the Witteberg quartzites with> 30% Cl.<br />

(d) In terms <strong>of</strong> the CaO : MgO ratio, MgO generally exceeds CaO.<br />

(el Waters are slightly acidic with a pH just under 7,0.<br />

(f) The waters are all very s<strong>of</strong>t.<br />

(gl Group E waters are those arising in sandstones and quartzitic rocks <strong>of</strong> the<br />

Witwatersrand System, the Pretoria quartzites, Waterberg sandstones, the Table<br />

Mountain Series in Natal and the Cape, and in the Old granite <strong>of</strong> the southern<br />

Transvaal.<br />

11.14.1 Some general observations regarding groundwater guality {according to Bond.<br />

19461<br />

(a) Ecca waters in northern Natal do not conform to any type.<br />

(b) The most saline waters in South Africa - excluding the Pondoland (Transkei) Dwyka<br />

springs which are rare - are those arising in the Old granite <strong>of</strong> the north west Cape<br />

which have a mean TDS concentration <strong>of</strong> nearly 7 000 mg r 1 •<br />

(cl The most alkaline waters in South Africa are those arising in the Upper Beaufort<br />

and Stormberg sediments, and in some <strong>of</strong> the Pilansberg alkali rocks.

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